Regional positive gravity anomaly over the Mississippi embayment

Details Regional positive gravity anomaly over the Mississippi embayment Regional positive gravity anomaly over the Mississippi embayment

Jul 1977

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1977georl...4..285c&link_type=abstract

Geophysical Research Letters, vol. 4, July 1977, p. 285-287.

Mathematics

Logic

Geological Surveys, Gravity Anomalies, Mississippi River (Us), Paleontology, Sedimentary Rocks, Seismology

Scientific paper

When gravity data are corrected for low-density sedimentary rocks, the positive gravity anomaly associated with the Mississippi embayment is seen to be continuous along the embayment. The continuity of the axial gravity anomaly suggests that a reversed seismic profile along the axis and a deep seismic reflection across it would yield crucial information on the crustal structure of the embayment.

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